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. 2020 Jan 27;11:522. doi: 10.1038/s41467-020-14411-z

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© The Author(s) 2020

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 1 — a Distribution of saturated hydraulic conductivity subdivided for soil-textural types (sand, sandy loam, silt and loam combined, and clay) for undisturbed samples only of the UNSODA database (Nemes et al.⁴⁶ and Børgesen et al.⁴⁷). b Hypothetical distributions of soil saturated hydraulic conductivity (K_s) obtainable from soil cores vs. rarely observed structured soil samples. The dashed line delimits the largest value of K_s related to texture. Solid lines are the medians of the two distributions. c Distribution of the ratio between structural and textural saturated conductivity K_s,str/K_s,tex subdivided for soil-textural types (data from Weynants et al.³⁹). The box length provides the interquartile range (IQR), the bottom of the box the 25th percentile (first quartile, q1), the top of the box the 75th percentile (third quartile, q3), and the horizontal line within the box the median value. The lower whisker corresponds to q1 − 1.5IQR and the upper whisker corresponds to q3 + 1.5IQR; outliers are plotted individually.